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zhu zhuang jie li de yan xing wei hua gang ban yan , xing cheng yu yue 9000 wan nian qian wan bai zuo ji guang xi fa xian da xing zhu zhuang jie li di mao
Pages: 50-53
Year: Issue:  4
Journal: NANFANG GUOTU ZIYUAN

Abstract: 最近,广西区域地质调查研究院的地质专家在广西岑溪市发现大型柱状节理地貌现象.经实地考察和岩石鉴定,专家认为该柱状节理的岩性为花岗斑岩,形成于约9000万年前晚白垩纪. 该大型柱状节理地貌,位于岑溪市大业镇以东约3公里的岑罗二级公路旁.这里是个废弃的采石场,其裸露的一根根排列极为规整的菱形石柱迭层并列,高约30米,连绵约有100多米宽,甚为壮观.
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